首页> 外文会议>2009 ISEST;International symposium on environmental science and technology >Responses of Phenol Oxidase Activity to Water Level Changes in Peatlands: Implications for Global Carbon Cycling
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Responses of Phenol Oxidase Activity to Water Level Changes in Peatlands: Implications for Global Carbon Cycling

机译:泥炭地苯酚氧化酶活性对水位变化的响应:对全球碳循环的影响

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Phenol oxidase is expected to play a “latch” role in the responses of carbon cycling in peatlands to global climate change. The effects of water level changes on phenol oxidase activity and phenolic substances were examined in two typical peatlands, bog and swamp, located in Hsiao Hsinganling, Heilongjiang province, north China. The results indicted the ratio of measured phenol oxidase activity to phenolics concentration is an effective index mark illustrating the impacts of water level changes on phenol oxidase involved carbon cycling processes. The responses of phenol oxidase activities to water level changes are subject to not only oxygen restrictions but also acidification/drought stress. For swamp, biogeochemical processes at upmost surface (0-10 cm) act as a pivotal role in responses of carbon cycling to water level changes. Nevertheless, biogeochemical responses in deeper bog peat (10-18 cm) to water level depression can not be neglected in assessing the impacts of moisture condition changes on enzyme-involved soil organic matter decomposition.
机译:在泥炭地碳循环对全球气候变化的响应中,酚氧化酶有望发挥“闩锁”作用。在中国北方黑龙江省小兴安岭的两个典型的泥炭地沼泽和沼泽中,研究了水位变化对酚氧化酶活性和酚类物质的影响。结果表明,测得的酚氧化酶活性与酚类浓度的比率是一个有效的指标,说明水位变化对涉及碳循环过程的酚氧化酶的影响。酚氧化酶活性对水位变化的响应不仅受氧限制,而且受酸化/干旱胁迫的影响。对于沼泽,在最高表面(0-10厘米)的生物地球化学过程在碳循环对水位变化的响应中起着举足轻重的作用。然而,在评估湿度条件变化对酶引起的土壤有机质分解的影响时,不能忽略深陷泥炭(10-18厘米)对水位下降的生物地球化学反应。

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